Velocity Anisotropy Of Two Deep Crystalline Samples

Using ultrasonic velocity measurements taken over a multiplicity of directions we show that samples exhibit weak to moderate anisotropy of seismic velocities. We further define the anisotropic geometry with high resolution scanning electron microscopy. Our data indicate that one sample, a granite...

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Main Authors: Mendelson, Jim, Toksoz, M. N.
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2012
Online Access:http://hdl.handle.net/1721.1/75149
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author Mendelson, Jim
Toksoz, M. N.
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Mendelson, Jim
Toksoz, M. N.
author_sort Mendelson, Jim
collection MIT
description Using ultrasonic velocity measurements taken over a multiplicity of directions we show that samples exhibit weak to moderate anisotropy of seismic velocities. We further define the anisotropic geometry with high resolution scanning electron microscopy. Our data indicate that one sample, a granite, is transversely anisotropic, and that the presence of fine to moderately fine microcracks is the most important factor effecting the velocities. We model the angular velocity dependence using 5 elastic constants and show that all 9 observed velocities fit these predictions to within 0.1 km/s. We are unable to obtain similar fits to a second sample, a mica-schist, in the same fashion. SEM observations indicate this rock displays orthorhombic symmetry. We made additional velocity measurements in order to calculate 9 elastic constants, and found that the predicted angular velocity dependence agreed much better with our velocity observations.
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spelling mit-1721.1/751492019-04-10T18:05:03Z Velocity Anisotropy Of Two Deep Crystalline Samples Mendelson, Jim Toksoz, M. N. Massachusetts Institute of Technology. Earth Resources Laboratory Mendelson, Jim Toksoz, M. N. Using ultrasonic velocity measurements taken over a multiplicity of directions we show that samples exhibit weak to moderate anisotropy of seismic velocities. We further define the anisotropic geometry with high resolution scanning electron microscopy. Our data indicate that one sample, a granite, is transversely anisotropic, and that the presence of fine to moderately fine microcracks is the most important factor effecting the velocities. We model the angular velocity dependence using 5 elastic constants and show that all 9 observed velocities fit these predictions to within 0.1 km/s. We are unable to obtain similar fits to a second sample, a mica-schist, in the same fashion. SEM observations indicate this rock displays orthorhombic symmetry. We made additional velocity measurements in order to calculate 9 elastic constants, and found that the predicted angular velocity dependence agreed much better with our velocity observations. Massachusetts Institute of Technology. Full Waveform Acoustic Logging Consortium Ente nazionale per l'energia elettrica 2012-12-03T18:30:47Z 2012-12-03T18:30:47Z 1989 Technical Report http://hdl.handle.net/1721.1/75149 Earth Resources Laboratory Industry Consortia Annual Report;1989-13 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Mendelson, Jim
Toksoz, M. N.
Velocity Anisotropy Of Two Deep Crystalline Samples
title Velocity Anisotropy Of Two Deep Crystalline Samples
title_full Velocity Anisotropy Of Two Deep Crystalline Samples
title_fullStr Velocity Anisotropy Of Two Deep Crystalline Samples
title_full_unstemmed Velocity Anisotropy Of Two Deep Crystalline Samples
title_short Velocity Anisotropy Of Two Deep Crystalline Samples
title_sort velocity anisotropy of two deep crystalline samples
url http://hdl.handle.net/1721.1/75149
work_keys_str_mv AT mendelsonjim velocityanisotropyoftwodeepcrystallinesamples
AT toksozmn velocityanisotropyoftwodeepcrystallinesamples